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新疆西准噶尔扎合金矿地质特征及成因
引用本文:辛存林,孙现辉,陈世伟,都卫东,魏明. 新疆西准噶尔扎合金矿地质特征及成因[J]. 兰州大学学报(自然科学版), 2012, 48(2): 48-52
作者姓名:辛存林  孙现辉  陈世伟  都卫东  魏明
作者单位:西北师范大学地理与环境科学学院,兰州,730070
基金项目:甘肃省科技支撑基金项目(1104FKCA116);甘肃省高等学校研究生导师科研项目(1101-07);兰州市科技计划基金项目(2011-2-89)
摘    要:扎合金矿位于准噶尔板块萨吾尔晚古生代岛弧区的中南段,矿体赋存于海西晚期—印支早期侵入的中性闪长岩岩体及围岩接触部位.矿区内发育北西向和北东向两组断裂.北西向断裂既是成矿热液运移的通道,也是金元素富集成矿的场所,岩体为金矿提供了成矿物质和部分热液.根据矿体产出地质特征,扎合金矿属构造蚀变岩型金矿床;据成矿作用分析,该金矿属中低温热液金矿床.

关 键 词:金矿  成因  扎合  西准噶尔

Geological characteristics and genesis of Zhahe gold deposit in western Junggar,Xinjiang
XIN Cun-lin , SUN Xian-hui , CHEN Shi-wei , DU Wei-dong , WEI Ming. Geological characteristics and genesis of Zhahe gold deposit in western Junggar,Xinjiang[J]. Journal of Lanzhou University(Natural Science), 2012, 48(2): 48-52
Authors:XIN Cun-lin    SUN Xian-hui    CHEN Shi-wei    DU Wei-dong    WEI Ming
Affiliation:School of Geography and Environment Sciences,Northwest Normal University,Lanzhou 730070
Abstract:Zhahe gold deposit is located in the middle-to-south part of the Sawuer late paleozoic island arc of the Junggar plate.Orebodies occurring in diorite invaded the late Hercy-early Indosinian and the surrounding area of diorite.Two groups of faults,i.e.the north-west and north-east faults,exist in the mining area.The north-west faults have been the migration channels of metallogenic hydrotherm and the ore-forming place for the concentration of gold elements.Magma provided the gold metallogenic material and part of hydrotherm. According to the geological characteristics of orebodies,Zhahe gold deposit belongs to the structural alerted-rock type.And a mineralization analysis showed that it is a medium-low temperature hydrothermal deposit.
Keywords:gold deposit  genesis  Zhahe  western Junggar
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